LESSON RAY OPTICS Introduction Note Ray of light Beam of light Reflection of Light by Spherical Mirrors Law of reflection Note:

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2 2 LESSON RAY OPTICS Introduction Electromagnetic radiation belonging to the region of the electromagnetic spectrum (wavelength of about 400 nm to 750 nm) is called light. Nature has endowed the human eye (retina) with the sensitivity to detect electromagnetic waves within this small range of the electromagnetic spectrum. It is mainly through light and the sense of vision that we know and interpret the world around us. There are two things that is easily identifiable with light 1. Light travels with enormous speed and 2. Light travels in a straight line. Its presently accepted value in vacuum is c = ms 1. For many purposes, it suffices to take c = ms 1. Note: (i). The speed of light in vacuum is the highest speed attainable in nature. (ii). The wavelength of light is very small compared to the size of ordinary objects that we encounter commonly, hence, it can be taken to be moving in a straight line Ray of light- A light wave can be considered to travel from one point to another, along a straight line joining them. The path is called a ray of light, Beam of light- A bundle of such rays constitutes a beam of light. In this chapter, we consider the phenomena of reflection, refraction and dispersion of light, using the ray picture of light. Using the basic laws of reflection and refraction, we shall study the image formation by plane and spherical reflecting and refracting surfaces. We then go on to describe the construction and working of some important optical instruments, including the human eye. Reflection of Light by Spherical Mirrors Law of reflection - The law of reflection by a plane mirror states that: (i) the angle of incidence (angle between incident ray and the normal to the mirror) equals the angle of reflection (angle between reflected ray and the normal). This law is also applied at every point on the surface of a spherical mirror. (ii) the incident ray, reflected ray and the normal to the reflecting surface at the point of incidence lie in the same plane. Note: These laws are valid at each point on any reflecting surface whether plane or curved. The normal in this case is to be taken as normal to the tangent to surface at the point of incidence. That is, the normal is along the radius, the line joining the centre of curvature of the mirror to the point of incidence. Terms associated with spherical mirrors Pole- The geometric centre of a spherical mirror is called its pole. Principal axis- The line joining the pole and the centre of curvature of the spherical mirror is known as the principal axis. Paraxial Rays- The rays that are incident at points close to the pole P of the mirror and make small angles with the principal axis are called paraxial rays.

3 3 Focus For Concave mirror When a parallel beam of light is incident on a concave mirror, at points close to the pole of the mirror, P, the reflected rays converge at a point F(principal focus of the mirror) on the axis for a concave mirror. For Convex mirror When a parallel beam of light is incident on a convex mirror, the reflected rays appear to diverge from a point F (principal focus of the mirror).the point F is called the principal focus of the mirror. Focal Length The distance between the focus F and the pole P of the mirror is called the focal length of the mirror. Focal Plane If the parallel paraxial (close to the principal axis) beam were incident making some angle with the axis, the reflected rays would converge (or appear to diverge) from a point in a plane through F normal to the axis. This is called the focal plane of the mirror. Derivation for focal length The distance between the focus F and the pole P of the mirror is called the focal length of the mirror, denoted by f. We now show that f = R/2, where R is the radius of curvature of the mirror. The geometry of reflection of an incident ray is shown in figure. At the point of incidence M, applying the laws of reflection MCP and MFP = 2 MD MD Now tanθ=, tan2θ= (for small, tan = CD FD and tan 2 = 2 ); thus we have MD =2 MD FD CD CD or FD = 2 Also for small the point D is very close to the point P. Therefore,

4 FD = f and CD = R; Equation (1) then gives F = R/2 Note: In this section P is the pole of the mirror 4 Sign Convention New Cartesian sign convention. (see figure) All distances are measured from the pole of the mirror or the optical center of the lense. The distances measured in the same direction as the incident light are taken as positive The distances measured in the direction opposite to the direction of incident light are taken as negative. The heights measured upwards (above x-axis) and normal to the principal axis of the mirror/lens are taken as positive. The heights measured downwards are taken as negative. The Mirror Equation Image of a point If the rays starting from a point meet at another point after reflection and or refraction, the point is called the image of the first point. Real Image The image is real if the rays actually converges at the point Virtual image - The image is virtual if the rays do not actually meet but appear to diverge from the point when produced backwards. Image of an object Take any two rays coming from an object, trace their paths, find their point of intersection and thus, obtain the image of the point. For convenience in application of geometry the following rays could be considered (i) The ray which is parallel to the principal axis. The reflected ray goes through the focus of the mirror. (ii) The ray passing through the centre of curvature of a concave mirror or appearing to pass through it for a convex mirror. The reflected ray simply retraces the path. (iii) The ray passing through the focus of the concave mirror or appearing to pass through (or directed towards) the focus of a convex mirror. The reflected ray is parallel to the principal axis. Figure gives the ray diagram showing the image (in this case, real) of an object formed by a concave mirror. Derivation of Mirror equation Mirror equation is the relation between the object distance (u), image distance (v) and the focal length (f). Using geometry the two right-angled triangles A'B'F and MPF are similar. (For paraxial rays, MP can be considered to be a straight line perpendicular to CP). Therefore, A'B' B'F MP PF

5 or A'B' B'F (1) AB PF The right angled triangles A B P and ABP are also similar. Therefore, A'B' B'P (2) AB BP B'P PF B'P Comparing Eqs. (1) and (2), we get (3) PF BP Equation (3) is a relation involving magnitudes of the distance. Applying sign conventions: B V = -v, VF = -f, BV = -u (4) v f v we get (5) f u or v f v f u (6) v u f This relation is known as the mirror equation Magnification (m) In triangles A'B'P & ABP, we have B'A' B'P BA BP with sign convention, this becomes h ' v h ' v h u h u 5 Image formation for different cases In this section we have derived the mirror equation, and the magnification formula, for the case of real, inverted image formed by a concave mirror only. It is to be noted here that with the proper use of sign convention, these equations are valid for all the cases of reflection by a spherical mirror (concave or convex) whether the image formed is real or virtual. Ray diagrams for image formations

6 6 The figures here show the ray diagrams for virtual image formed by a concave and convex mirror. It can be easily verified that the equations derived above are valid for these cases also Refraction When light travels from one medium to another, it changes the direction of its path at the interface of the two media. This is called refraction of light. Laws of refraction The following are the laws of refraction (i). The incident ray, the refracted ray and the normal to the interface at the point of incidence, all lie in the same plane. (ii). The ratio of the sine of the angle of incidence to the sine of angle of refraction is constant. Note: the angles of incidence (i) and refraction (r) are the angles that the incident and refracted rays make with the normal. sin i n21 sin r (where n 2l is a constant, called the refractive index of the second medium with respect to the first medium and is independent of the angle of incidence. ) Snell's law of refraction sin i Equation n 21, is the Snell s law of refraction sin r If n 21 > 1, r < i, that is, the refracted ray bends towards the normal. The medium 2 is said to be optically denser than medium 1. On the other hand, if n 21 < 1, r > i, the refracted ray bends away from the normal. n2 We have n21 n1 1 The equation shows that n21 and n 32 = n 31 n 12 n 12 Note: Optical density should not be confused with mass density, which is mass per unit volume. It is possible that mass density of an optically denser medium may be less than that of an optically rarer medium (optical density is the ratio of the speed of light in two media). For example in case of turpentine and water, the mass density of turpentine is less than that of water but its optical density is higher. Refraction for a rectangular glass slab Some elementary results based on the laws of refraction follow immediately. For a rectangular slab, refraction takes place at two interfaces (air-glass and glass-air). It is easily seen from the figure that r 2 = i 1, i.e., the emergent ray is parallel to the incident ray i.e. there is no deviation, but it does suffer lateral

7 displacement/shift with respect to the incident ray. 7 Refraction for a water tank Another familiar observation is that the bottom of a tank filled with water appears to be raised (as shown in the figure). For viewing near the normal direction, it can be shown that the apparent depth (h 1 ) is real depth (h 2 ) divided by the refractive index of the medium (water). Refraction for a water h 2(real depth) tank formula - h1 Refraction of light through the atmosphere It is because of the phenomenon of refraction that the sun is visible a little before the actual sunrise and until a little after the actual sunset due to refraction of light through the atmosphere. The refractive index of air with respect to vacuum is The apparent shift in the direction of the sun is by about half a degree and the corresponding time difference between actual sunset and apparent sunset is about 2 minutes. The apparent flattening (oval shape) of the sun at sunset and sunrise is also due to the same phenomenon. Note: 1. Actual sunrise means the actual crossing of the horizon by the sun. 2. The figure is highly exaggerated to show the effect. Total Internal Reflection

8 8 When light travels from an optically denser medium to a rarer medium at the interface, it is partly reflected back into the same medium and partly refracted to the second medium. This reflection is called the internal reflection. Let us consider the following when the light goes from the denser to rarer medium (as shown in the figure): 1. When a ray of light enters from a denser medium to a rarer medium, it bends away from the normal, for example, the ray AO 1 B in the figure. 2. The incident ray AO 1 is partially reflected (O 1 C) and partially transmitted (O 1 B) or refracted, the angle of refraction (r) being larger than the angle of incidence (i). 3. As the angle of incidence increases, so does the angle of refraction, till for the ray AO 3, the angle of refraction is 2 4. The refracted ray is bent so much away from the normal that it grazes the surface at the interface between the two media. This is shown by the ray AO 3 D in the figure. 5. If the angle of incidence is increased still further (e.g., the ray AO 4 ), refraction is not possible, and the incident ray is totally reflected. This is called total internal reflection. Some noteworthy points while taking into consideration the total internal refraction are: light When light gets reflected by a surface, normally some fraction of it gets transmitted. The reflected ray, therefore, is always less intense than the incident ray, howsoever smooth the reflecting surface may be. In total internal reflection, on the other hand, no transmission of takes place. The angle of incidence corresponding to an angle of refraction 90º, say AO 3 N, is called the critical angle (i c ) for the given pair of media. We see from Snell s law that if the relative refractive index is less than one then, since the maximum value of sin r is unity, there is an upper limit to the value of sin i for which the law can be satisfied, that is, i = i c such that sini c = n 21 For values of i larger than i c, Snell s law of refraction cannot be satisfied, and hence no refraction is possible. The refractive index of denser medium 2 with respect to rarer medium 1 will be 1 n 12 = sin(i ). c

9 9 Examples and uses of total internal reflection Mirage: On hot summer days, the air near the ground may become hotter than air further up. The refractive index of air increases with its density. Hotter air is less dense, and so has smaller refractive index than cooler air. So, light from a tall object such as a tree passes through a medium whose refractive index decreases towards the ground. Thus a ray of light from such an object gets bent and is totally internally reflected. The observer naturally assumes that light is being reflected from the ground, say, by a pool of water near the tall object. Such inverted images of distant high objects cause the optical illusion called a mirage, specially common in hot deserts. Diamond: Total internal reflection is the main cause of the brilliance of diamonds. Its critical angle (24.4 ) is very small, so that once light gets into diamond, it is very likely to be totally reflected internally. By cutting the diamond suitably, multiple internal reflections can be made to occur. Prism: Prisms make use of total internal reflection to bend light by 90 or by 180, or to invert images without changing their size.

10 10 Optical fibres: Optical fibres consist of many long high quality composite glass/quartz fibres. Each fibre consists of a core and cladding. The refractive index of the material of the core is higher than that of the cladding. A bundle of optical fibres can be put to several uses. It can be used as a 'light pipe' in medical and optical examination. It can also be used for optical signal transmission. Optical fibres have also been used for transmitting and receiving electrical signals which are converted to light by suitable transducers. The main requirement is that there should be very little absorption of light as it has to travel long distances, inside the optical fibre. Refraction at a Spherical Surface Any small part of a spherical surface can be regarded as planar and the same laws of refraction can be applied at every point on the surface. The normal at the point of incidence is perpendicular to the tangent plane to the surface at that point and, therefore, passes through the centre of curvature of the surface. Consider refraction by a single spherical surface as shown in the figure. The figure shows the geometry of formation of image I of an object point O on the principal axis of the spherical surface with centre of curvature C, and radius of curvature R. The rays are incident from a medium of refractive index n 1 to another of refractive index n 2. We take the aperture (or the lateral size) of the surface to be small compared to other distances involved, so that small angle approximation can be made, wherever appropriate. In particular, NM will be taken to be nearly equal to the length of the perpendicular from N to the principal axis. We have MN tan NOM NOM (for small angles), OM MN tan NCM NCM (for small angles), MC MN tan NIM NIM (for small angles). MI Now, for NOC, i is the exterior angle. Therefore, i NOM NCM MN MN OM MC (1) Similarly, r NCM NIM MN MN i.e., r MC MI (2) Now, by Snell s law n 1 sin i = n 2 sin r Or for small angles n 1 i = n 2 r Substituting i and r from Eqs. (1) and (2), we get

11 11 n n 1 2 n2 n1 (3) OM MI MC Here, OM, MI, MC represent magnitudes of distances. Applying the New Cartesian sign convention, OM = -u, MI = +v, MC = +R. We get n2 n1 n2 n1 v u R Refraction by a Lens Lens - A thin lens is a transparent optical medium bounded by two spherical surfaces. Applying the formula for image formation by a single spherical surface successively at the two surfaces of a lens, we obtain the thin lens formula and the lens maker s formula. The image formation can be seen in terms of two steps: The first refracting surface forms the image I 1 of the object O. The image I l acts as a virtual object for formation of image I by the second surface. n2 n1 n2 n1 Applying Eq. to the first v u R interface ABC, we get: n1 n2 n2 n1 (1) OB BI1 BC1 A similar procedure applied to the second interface ADC gives, n2 n1 n2 n1 (2) DI1 DI DC2 For a thin lens, BI 1 = DI 1. Adding Equations (1) and (2) we get: n1 n1 1 1 (n2 n 1) (3) OB DI BC1 DC2 Special case If the object is at infinity, OB = and I is at the focus of the lens so that DI = f, the focal length of the lens (f positive for a convex lens). Thus. Eq. (3) gives n1 1 1 (n2 n 1) f BC1 DC2 (4) By the sign convention, BC 1 = + R 1, DC 2 = -R 2 So we get: (n21 1) (lens maker's formula) (5) f R1 R 2

12 12 This equation is useful to design lenses of desired focal length using surfaces of suitable radii of curvature. From Eqs. (3) and (4) we get n1 n1 n1 OB DI f Again, in the thin lens approximation, B and D are both close to the optical centre of the lens. Applying the sign convention, OB = - u, DI = +v, we get (thin lens formula) v u f Note: This formula is true for a concave lens also. In that case R 1 is negative, R 2 positive and therefore f is negative. Image of object through the lens To find the image of an object by a lens, we can, in principle, take any two rays coming from an object point and trace their paths using the laws of refraction and find the point where the refracted rays meet (or appear to meet). In practice, however, it is convenient to choose any two of the following rays: (i) A ray from the object parallel to the principal axis of the lens after refraction passes through the second principal focus F' (in a convex lens) or appears to diverge (in a concave lens) from the first principal focus F. (ii) A ray of light, passing through the optical centre of the lens, emerges without any deviation after refraction. (iii) A ray of light passing through the first principal focus (for a convex lens) or appearing to meet at it (for a concave lens) emerges parallel to the principal axis after refraction. The figures illustrate these rules for a convex and a concave lens. Magnification (m) Magnification produced by a lens is defined as the ratio of the size of the image to that of the object. The size of the object h is always taken to be positive, but image size h is positive for erect image and negative for an inverted image. Proceeding in the same way as for spherical mirrors, it is easily seen that for a lens h ' v m h u Thus, for erect (and virtual) image formed by a convex or concave lens, m is positive, while for an inverted (and real) image, m is negative. Power of a lens Power of a lens is a measure of the convergence or divergence, which a lens introduces in the light falling on it. Clearly, a lens of shorter focal length bends the incident light more, while converging it in case of a convex lens and diverging it in case of a concave lens. The power P of a lens is defined as the

13 13 tangent of the angle by which it converges or diverges a beam of light falling at unit distant from the optical center. h tan ; f 1 if h = 1 then tan = f 1 or = for small value of. f 1 Thus, p= f The SI unit for power of a lens is dioptre (D): 1D = 1m 1. The power of a lens of focal length of 1 metre is one dioptre. Power of a lens is positive for a converging lens and negative for a diverging lens. Thus, when an optician prescribes a corrective lens of power D, the required lens is a convex lens of focal length + 40 cm. A lens of power of 4.0 D means a concave lens of focal length 25 cm. Combination of Thin Lenses in Contact Two lenses in contact Consider two lenses A and B of focal length f 1 and f 2 placed in contact with each other. Since the lenses are thin, we take the optical centres of the lenses to be coincident. For the image formed by the first lens A, We get (1) v1 u f1 For the image formed by the second lens B, we get (2) v v1 f2 Adding Eqs (1) and (2), we get v u f1 f2 If the two lens-system is regarded as equivalent to a single lens of focal length f, we have where v u f f f1 f2 n lenses in contact The equation is given as where... v u f f f1 f2 f3 Power is given as P = P 1 + P 2 + P 3 + where P is the net power of the lens combination. Note- Lens combination helps to increase the magnification and sharpness of the image. Magnification The total magnification m of the combination is a product of magnification (m 1, m 2, m 3,.,) of individual lenses: thus m = m 1 m 2 m 3..

14 14 Refraction through a Prism Figure shows the passage of light through a prism ABC. (i). The angles of incidence and refraction at the first face AB are i and r 1. (ii). The angle of incidence (from glass to air) at the second face AC is r 2 and the angle of refraction or emergence is e. (iii). The angle between the emergent ray RS and incident ray PQ is called the angle of deviation,. In the quadrilateral AQNR, two of the angles (at the vertices Q and R) are right angles. Therefore, the sum of the other angles of the quadrilateral is 180. A QNR 180 from the triangle QNR, r 1 r 2 QNR 180 Comparing these two equations, we get r 1 + r 2 = A (1) The total deviation is the sum of deviations at the two faces: = (i r 1 ) + (e r 2 ) i.e. = i + e - A (2) Fig. (a) Refraction through prism Plot between Angle of deviation and angle of incidence The angle of deviation depends on the angle of incidence. A plot between the angle of deviation and angle of incidence is shown in Fig. (b). It can be seen that, in general, any given value of δ, except for i = e, corresponds to two values i and hence of e. This, in fact, is expected from the symmetry of i and e in Eq. (2), i.e., δ remains the same if i and e are interchanged. Physically, this is related to the fact that the path of ray in Fig. (a) can be traced back, resulting in the same angle of deviation. At the minimum deviation D m, the refracted ray inside the prism becomes parallel to its base. We have δ = D m, i = e which implies r 1 = r 2. Equation (1) gives 2r = A or r = A (3) 2 In the same way, Eq. (2) gives D m = 2i A, or i = A D m (4) 2 The refractive index of the prism is A Dm sin n 2 2 n21 (5) n A 1 sin 2 The angles A and D m can be measured experimentally. Equation (5) thus provides a method of determining refractive index of the material of the prism. For a small angle prism, i.e., a thin prism, D m is also very small, and we get Fig. (b) Plot of angle of deviation () versus angle of incidence (i) for a triangular prism.

15 A Dm A D 15 sin m 2 n 2 21 A A sin 2 2 D m = (n 21 1)A This implies that a thin prisms do not deviate light much. Dispersion by a Prism Dispersion is the splitting of light into its component colours and the pattern of colour components of light is called its spectrum. (i). When a narrow beam of sunlight is incident on a glass prism, the emergent light is seen to be consisting of several colours. (ii). The different component colours in sequence are: violet, indigo, blue, green, yellow, orange and red (given by the acronym VIBGYOR). The red light bends the least, while the violet light bends the most. White light itself consists of colours which are separated by the prism. (iii). Colour is associated with wavelength of light. In the visible spectrum, red light is at the long wavelength end (~700 nm) while the violet light is at the short wavelength end (~ 400 nm). (iv). Dispersion takes place because the refractive index of medium for different colours is different. Red light bends less than violet. Note: Thick lenses could be assumed as made of many prisms, therefore, thick lenses show chromatic aberration due to dispersion of light. Some natural phenomena due to sunlight The interplay of light with things around us gives rise to several beautiful phenomena. The spectacle of colour that we see around us all the time is possible only due to sunlight. The blue of the sky, white clouds, the redhue at sunrise and sunset, the rainbow, the brilliant colours of some pearls, shells, and wings of birds, are just a few of the natural wonders we are used to. We describe some of them here from the point of view of physics. The rainbow The rainbow is an example of the dispersion of sunlight by the water drops in the atmosphere. This is a phenomenon due to combined effect of dispersion, refraction and reflection of sunlight by spherical water droplets of rain. The conditions for observing a rainbow are that the sun should be

16 16 shining in one part of the sky (say near western horizon) while it is raining in the opposite part of the sky (say eastern horizon). An observer can therefore see a rainbow only when his back is towards the sun. In order to understand the formation of rainbows, consider the following: 1. The sunlight is first refracted as it enters a raindrop (as in the figure (a)), which causes the different wavelengths (colours) of white light to separate. Longer wavelength of light (red) are bent the least while the shorter wavelength (violet) are bent the most. 2. Next, these component rays strike the inner surface of the water drop and get internally reflected if the angle between the refracted ray and normal to the drop surface is greater than the critical angle (48º, in this case). 3. The reflected light is refracted again as it comes out of the drop as shown in the figure. It is found that the violet light emerges at an angle of 40º related to the incoming sunlight and red light emerges at an angle of 42º. For other colours, angles lie in between these two values. Primary rainbow- The figure (b) explains the formation of primary rainbow. We see that red light from drop 1 and violet light from drop 2 reach the observers eye. The violet from drop 1 and red light from drop 2 are directed at level above or below the observer. Thus the observer sees a rainbow with red colour on the top and violet on the bottom. Thus, the primary rainbow is a result of threestep process, that is, refraction, reflection and refraction.

17 17 Secondary Rainbow- When light rays undergoes two internal reflections inside a raindrop, instead of one as in the primary rainbow, a secondary rainbow is formed as shown in the figure (c). It is due to four-step process. The intensity of light is reduced at the second reflection and hence the secondary rainbow is fainter than the primary rainbow. Further, the order of the colours is reversed in it as is clear from the figure (c). Scattering of light in earth s atmosphere As the sunlight travels through the earth s atmosphere, it gets scattered (changes its direction) by the atmospheric particles. The amount of scattering is inversely proportional to the fourth power of the wavelength. This is known as Rayleigh scattering The various colours observed around us such as the blue colour of sky, white colour of clouds, red colour of setting sun etc. are because of scattering. Blueness of sky Light of shorter wavelengths is scattered much more than the light of longer wavelengths. Hence, the bluish colour predominates in a clear sky, since blue has a shorter wavelength than red and is scattered much more strongly. In fact, violet gets scattered even more than blue, because of a even shorter wavelength. But our eyes are more sensitive to blue than violet, hence we see the sky as blue. Whiteness of clouds Large particles like dust and water droplets present in the atmosphere behave differently. The relevant quantity here is the relative size of the wavelength of light, and the scatterer (of typical 1 size, say, a). For a, one has Rayleigh scattering which is proportional to 4. For a >>, i.e., large scattering objects (for example, raindrops, large dust or ice particles) this is not true; all wavelengths are scattered nearly equally. Thus clouds which have droplets of water, with a>>,are generally white. Reddishness observed in sun and moon At sunset or sunrise, the sun s rays have to pass through a larger distance in the atmosphere (as shown in figure). Most of the blue and other shorter wavelengths are removed by scattering. The least scattered light reaching our eyes, therefore, the sun looks reddish. This explains the reddish appearance of the sun and full moon The Microscope Simple microscope A simple magnifier or microscope is a converging lens of small focal length as shown in the figure. In order to use such a lens as a microscope, the lens is held near the object, one focal length away or less, and the eye is positioned close to the lens on the other side. The idea is to get an erect, magnified and virtual image of the

18 18 object at a distance so that it can be viewed comfortably, i.e., at 25 cm or more. If the object is at a distance f, the image is at infinity. However, if the object is at a distance slightly less than the focal length of the lens, the image is virtual and closer than infinity. Although the closest comfortable distance for viewing the image is when it is at the near point (distance D 25 cm), it causes some strain on the eye. Therefore, the image formed at infinity is often considered most suitable for viewing by the relaxed eye. We show both cases, the first in Fig. (a), and the second in Fig. (b) and (c). Magnification by microscope The linear magnification m, for the image formed at the near point D, by a simple microscope can be obtained by using the relation v 1 1 v m v 1 u v f f Now according to our sign convention, v is negative, and is equal in magnitude to D. Thus, the magnification is D m1 f Since D is about 25 cm, to have a magnification of six, one needs a convex lens of focal length, f = 5 cm. Note that m = h /h where h is the size of the object and h the size of the image. This is also the ratio of the angle subtended by the image to that subtended by the object, if placed at D for comfortable viewing. (Note that this is not the angle actually subtended by the object at the eye, which is h/u.) What a single-lens simple magnifier achieves is that it allows the object to be brought closer to the eye than D. Image at infinity We will now find the magnification when the image is at infinity. In this case we will have to obtain the angular magnification. Suppose the object has a height h. The maximum angle it can subtend, and be clearly visible (without a lens), is when it is at the near point, i.e., a distance D. The angle h subtended is then given by tan 0 0 D We now find the angle subtended at the eye by the image when the object is at u. From the relations h ' v m h u We have the angle subtended by the image h ' h v h tan i. v v u u The angle subtended by the object, when it is at u = f h i f As is clear from Fig. The angular magnification is, therefore i D m 0 f

19 19 This is one less than the magnification when the image is at the near point, but the viewing is more comfortable and the difference in magnification is usually small. In subsequent discussions of optical instruments (microscope and telescope) we shall assume the image to be at infinity. Compound microscope A simple microscope has a limited maximum magnification ( 9) for realistic focal lengths. For much larger magnifications, one uses two lenses, one compounding the effect of the other. This is known as a compound microscope. A schematic diagram of a compound microscope is shown in the figure. The lens nearest the object, called the objective, forms a real, inverted, magnified image of the object. This serves as the object for the second lens, the eyepiece, which functions essentially like a simple microscope or magnifier, produces the final image, which is enlarged and virtual. The first inverted image is thus near (at or within) the focal plane of the eyepiece, at a distance appropriate for final image formation at infinity, or a little closer for image formation at the near point. Clearly, the final image is inverted with respect to the original object. We now obtain the magnification due to a compound microscope. The ray diagram of Figure shows that the (linear) magnification due to the objective, namely h /h, equals. h L mo h f0 where we have used the result h h tan f0 L Here h is the size of the first image, the object size being h and f o being the focal length of the objective. The first image is formed near the focal point of the eyepiece. The distance L, i.e., the distance between the second focal point of the objective and the first focal point of the eyepiece (focal length f e ) is called the tube length of the compound microscope. Magnification As the first inverted image is near the focal point of the eyepiece, we use the result from the discussion above for the simple microscope to obtain the (angular) magnification me due to it, when the final image is formed at the near point, is D me 1 f e When the final image is formed at infinity, the angular magnification due to the eyepiece is m e = (D/f e ) Image at infinity Thus, the total magnification when the image is formed at infinity, is L D m mome f0 fe Note:

20 20 To achieve a large magnification of a small object (hence the name microscope), the objective and eyepiece should have small focal lengths. In practice, it is difficult to make the focal length much smaller than 1 cm. Also large lenses are required to make L large. Example: For an objective with f o = 1.0 cm, and an eyepiece with focal length f e = 2.0 cm, and a tube length of 20 cm, the magnification is L D m mome fo fo = Various other factors such as illumination of the object, contribute to the quality and visibility of the image. In modern microscopes, multicomponent lenses are used for both the objective and the eyepiece to improve image quality by minimising various optical aberrations (defects) in lenses. Telescope The telescope is used to provide angular magnification of distant objects (as shown in Figure). It also has an objective and an eyepiece. But here, the objective has a large focal length and a much larger aperture than the eyepiece. Light from a distant object enters the objective and a real image is formed in the tube at its second focal point. The eyepiece magnifies this image producing a final inverted image. Magnification of telescope The magnifying power m is the ratio of the angle β subtended at the eye by the final image to the angle α which the object subtends at the lens or the eye. Hence h fo fo m. fe h fe In this case, the length of the telescope tube is f o + f e. Note: Terrestrial telescopes have, in addition, a pair of inverting lenses to make the final image erect. Refracting telescope Refracting telescopes can be used both for terrestrial and astronomical observations. Example: Consider a telescope whose objective has a focal length of 100 cm and the eyepiece a focal length of 1 cm. The magnifying power of this telescope is m = 100/1 = 100. Let us consider a pair of stars of actual separation 1 (one minute of arc). The stars appear as though they are separated by an angle of = 100 =1.67º. Some other noteworthy points regarding refracting telescopes are: The main considerations with an astronomical telescope are its light gathering power and its resolution or resolving power. The former clearly depends on the area of the objective. With larger diameters, fainter objects can be observed. The resolving power, or the ability to observe two objects distinctly, which are in very nearly the same direction, also depends on the diameter of the objective. So, the desirable aim in optical telescopes is to make them with objective of large diameter.

21 21 The largest lens objective in use has a diameter of 40 inch (~1.02 m). It is at the Yerkes Observatory in Wisconsin, USA. Reflecting telescopes Very big lenses tend to be very heavy and therefore, difficult to make and support by their edges. Further, it is rather difficult and expensive to make such large sized lenses which form images that are free from any kind of chromatic aberration and distortions. For these reasons, modern telescopes use a concave mirror rather than a lens for the objective. Telescopes with mirror objectives are called reflecting telescopes. Advatages -They have several advantages. 1. There is no chromatic aberration in a mirror. 2. If a parabolic reflecting surface is chosen, spherical aberration is also removed. 3. Mechanical support is much less of a problem since a mirror weighs much less than a lens of equivalent optical quality, and can be supported over its entire back surface, not just over its rim. Cassegrain telescope One obvious problem with a reflecting telescope is that the objective mirror focusses light inside the telescope tube. One must have an eyepiece and the observer right there, obstructing some light (depending on the size of the observer cage). This is what is done in the very large 200 inch (~5.08 m) diameters, Mt. Palomar telescope, California. The viewer sits near the focal point of the mirror, in a small cage. Another solution to the problem is to deflect the light being focussed by another mirror. One such arrangement using a convex secondary mirror to focus the incident light, which now passes through a hole in the objective primary mirror, is shown in Fig. This is known as a Cassegrain telescope, after its inventor. It has the advantages of a large focal length in a short telescope. Note: The largest telescope in India is in Kavalur, Tamil Nadu. It is a 2.34 m diameter reflecting telescope (Cassegrain). It was ground, polished, set up, and is being used by the Indian Institute of Astrophysics, Bangalore. The largest reflecting telescopes in the world are the pair of Keck telescopes in Hawaii, USA, with a reflector of 10 metre in diameter.